REFINEMENT OF ENTHALPY MEASUREMENT OF MGSIO3 PEROVSKITE AND NEGATIVE PRESSURE-TEMPERATURE SLOPES FOR PEROVSKITE-FORMING REACTIONS

Authors
Citation
M. Akaogi et E. Ito, REFINEMENT OF ENTHALPY MEASUREMENT OF MGSIO3 PEROVSKITE AND NEGATIVE PRESSURE-TEMPERATURE SLOPES FOR PEROVSKITE-FORMING REACTIONS, Geophysical research letters, 20(17), 1993, pp. 1839-1842
Citations number
27
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
00948276
Volume
20
Issue
17
Year of publication
1993
Pages
1839 - 1842
Database
ISI
SICI code
0094-8276(1993)20:17<1839:ROEMOM>2.0.ZU;2-O
Abstract
Enthalpy for MgSiO3 orthopyroxene-perovskite transition at 298 K was m easured by differential drop-solution calorimetry. Based on four measu rements of MgSiO3 perovskite, the DELTAH-degrees 298 of 102.2+/-2.5 kJ /mol was more precisely determined than that in the previous study. Th e enthalpies of transitions from MgSiO3 ilmenite to perovskite and fro m Mg2SiO4 spinel to perovskite + periclase were calculated to be 43.2/-5.0 and 86.1+/-3.6 kJ/mol, respectively. The boundaries of these tra nsitions were calculated using the above data together with physical p roperties of relevant phases, including recently determined properties of perovskite: heat capacity, entropy, and temperature dependence of bulk modulus. The calculated P-T slopes for the ilmenite-perovskite tr ansition and the spinel dissociation are -3.4+/-2 and -3+/-1 MPa/K, re spectively. The tatter slope may suggest that the upper and lower mant le convect separately but intermittent mixing occurs between them.